Pub Date : 2015-06-03DOI: 10.1127/PALA/304/2015/77
J. Sandoval, G. Martínez, S. Ureta
{"title":"Toarcian-Aalenian Erycitinae, Ammonitida, of the westernmost Tethys (southern Spain): taxonomical and phylogenetical implications","authors":"J. Sandoval, G. Martínez, S. Ureta","doi":"10.1127/PALA/304/2015/77","DOIUrl":"https://doi.org/10.1127/PALA/304/2015/77","url":null,"abstract":"","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"2 1","pages":"77-119"},"PeriodicalIF":2.7,"publicationDate":"2015-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73305023","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2014-12-23DOI: 10.1127/PALA/303/2014/137
Detlef Thies, J. Vespermann, Jutta Solcher
Two new Late Triassic shark species (Synechodus seinstedtensis sp. nov., Parascylloides turnerae gen. nov. sp. nov.) belonging to the extinct order Synechodontiformes Duffin & Ward, 1993 (Chondrichthyes, Elasmobranchii, Neoselachii) are described on isolated oral teeth from Rhaetic deposits of North Germany and England.The term “polyhemiaulacorhize” is introduced for the synechodontiform type of root architecture in order to replace the misleading term “pseudopolyaulacorhize”. The teeth of Parascylloides turnerae gen. nov. sp. nov. were identified previously as symphyseals or parasymphyseals of Rhomphaiodon minor (Agassiz, 1837). They are considered here as belonging to a different, new species because of their frequency and their morphological differences to other Triassic neoselachian teeth. The teeth of both new species show a triple-layered enameloid microstructure consisting of an external shiny-layered enameloid (SLE), a middle parallel-bundled enameloid (PBE) and an internal tangled-bundled enameloid (TBE). In Synechodus seinstedtensis sp. nov. the PBE contains probably radial bundles of apatite cristallites whereas these are lacking in the PBE of Parascylloides turnerae gen. nov. sp. nov.. The systematical significance of the presence or absence of radial bundles in the PBE remains unclear. Zusammenfassung Anhand von Zähnen aus obertriaszeitlichen Rhät-Ablagerungen von Norddeutschland und England werden zwei neue Haiarten (Synechodus seinstedtensis sp. nov., Parascylloides turnerae gen. nov. sp. nov.) aus der ausgestorbenen Ordnung Synechodontiformes Duffin&Ward, 1993 (Chondrichthyes, Elasmobranchii, Neoselachii) beschrieben. Für die Charakterisierung derWurzelmorphologie synechodontiformer Zähne wird der Begriff „polyhemiaulacorhiz“ an Stelle des irreführenden älteren Terminus „pseudopolyaulacorhiz“ eingeführt. Die Zähne von Parascylloides turnerae gen. nov. sp. nov. wurden zuvor als Symphysenoder Parasymphysenzähne von Rhomphaiodon minor (Agassiz, 1837) angesprochen, werden hier jedoch aufgrund ihrer Häufigkeit und morphologischen Eigenart einer neuen Haiart zugeordnet. Der Zahnschmelz ist in beiden neuen Arten dreilagig aufgebaut und besteht aus einer äußeren Glanzschicht (SLE), einemmittleren parallelfaserigen Schmelz (PBE) und einem inneren wirrfaserigen Schmelz (TBE). Der parallelfaserige Schmelz zeigt in beiden Arten vertikale, oberflächenparallele Fasern aus Apatit-Kristalliten. Während im PBE von Synechodus seinstedtensis sp. nov. wahrscheinlich auch radiale Faserzüge vorhanden sind, fehlen diese im PBE von Parascylloides turnerae gen. nov. sp. nov. Die systematische Bedeutung des Vorhandenseins oder Fehlens von radialen Faserzügen im PBE, ein Phänomen, das auch bei anderen triassischen Neoselachiern beobachtet werden kann, bleibt unklar.
两个新的晚三叠世鲨鱼物种(Synechodus seinstedtensis sp. nov., Parascylloides turnerae gen. nov.)属于已灭绝的Synechodontiformes Duffin & Ward, 1993 (Chondrichthyes, Elasmobranchii, Neoselachii)在德国北部和英格兰Rhaetic沉积物的分离口腔牙齿上被描述。为了取代“伪多牙根”这一误导性的术语,“多牙根”一词被引入到共齿状根结构类型中。Parascylloides turnerae gen. nov. sp. nov.的牙齿以前被鉴定为Rhomphaiodon minor的联合或副联合(Agassiz, 1837)。它们被认为属于一个不同的新物种,因为它们的频率和形态与其他三叠纪新塞拉奇齿不同。这两个新物种的牙齿均呈三层状的类牙釉质微观结构,包括外部亮层类牙釉质(SLE)、中间平行束状类牙釉质(PBE)和内部缠结束状类牙釉质(TBE)。在Synechodus seinstedtensis sp. 11 .的PBE中可能含有放射状的磷灰石晶体束,而在Parascylloides turnerae gen. 11 . sp. 11 . 11 .中则缺乏。放射状束在PBE中存在或不存在的系统意义尚不清楚。zusmenfassung Anhand Zähnen aus obertriaszeitlichen Rhät-Ablagerungen von Norddeutschland and England werden zwei neue haarten (Synechodus seinstedtensis sp. 11, parascylides turnerae gen. 11 . sp. 11 .) aus der ausgestorbenen Ordnung Synechodontiformes Duffin&Ward, 1993 (chondrichthes, Elasmobranchii, Neoselachii) beschrieben。 die Charakterisierung derWurzelmorphologie synnechodontiformer Zähne wird der Begriff“polyhemaulacorhiz”和Stelle des irrefhrenden älteren Terminus“pseudpolyaulacorhiz”eingef hrt。Die Zähne von Parascylloides turnerae gen. nov. sp. nov. wurden zuvor als Symphysenoder Parasymphysenzähne von Rhomphaiodon minor (Agassiz, 1837) angesprochen, werden hier jedoch aufgrund irer Häufigkeit and morphologischen Eigenart einer neuen haart zugeordnet。Der Zahnschmelz ist in been neuen Arten dreilagig aufgebaut and bestebest aus einer äußeren Glanzschicht (SLE), einemmitleren parallelfaserigen Schmelz (PBE)和einem innerirfaserigen Schmelz (TBE)。Der parallelfaserige Schmelz height in en Arten vertikale, oberflächenparallele Fasern aus Apatit-Kristalliten。Während im PBE von synnechodus seinstedtensis sp. 11 . wahrscheinlich auch radiale faserz ge vorhanden sind, fehlen diese im PBE von parascyloides turnerae gen. 11 . sp. 11 . Die systematische Bedeutung des Vorhandenseins oder Fehlens von radialen faserz gen im PBE, ein Phänomen, das auch bei anderen triassischen neselachiern bebacachtet werden kann, bleibt unklar。
{"title":"Two new neoselachian sharks (Elasmobranchii, Neoselachii, Synechodontiformes) from the Rhaetian (Late Triassic) of Europe","authors":"Detlef Thies, J. Vespermann, Jutta Solcher","doi":"10.1127/PALA/303/2014/137","DOIUrl":"https://doi.org/10.1127/PALA/303/2014/137","url":null,"abstract":"Two new Late Triassic shark species (Synechodus seinstedtensis sp. nov., Parascylloides turnerae gen. nov. sp. nov.) belonging to the extinct order Synechodontiformes Duffin & Ward, 1993 (Chondrichthyes, Elasmobranchii, Neoselachii) are described on isolated oral teeth from Rhaetic deposits of North Germany and England.The term “polyhemiaulacorhize” is introduced for the synechodontiform type of root architecture in order to replace the misleading term “pseudopolyaulacorhize”. The teeth of Parascylloides turnerae gen. nov. sp. nov. were identified previously as symphyseals or parasymphyseals of Rhomphaiodon minor (Agassiz, 1837). They are considered here as belonging to a different, new species because of their frequency and their morphological differences to other Triassic neoselachian teeth. The teeth of both new species show a triple-layered enameloid microstructure consisting of an external shiny-layered enameloid (SLE), a middle parallel-bundled enameloid (PBE) and an internal tangled-bundled enameloid (TBE). In Synechodus seinstedtensis sp. nov. the PBE contains probably radial bundles of apatite cristallites whereas these are lacking in the PBE of Parascylloides turnerae gen. nov. sp. nov.. The systematical significance of the presence or absence of radial bundles in the PBE remains unclear. Zusammenfassung Anhand von Zähnen aus obertriaszeitlichen Rhät-Ablagerungen von Norddeutschland und England werden zwei neue Haiarten (Synechodus seinstedtensis sp. nov., Parascylloides turnerae gen. nov. sp. nov.) aus der ausgestorbenen Ordnung Synechodontiformes Duffin&Ward, 1993 (Chondrichthyes, Elasmobranchii, Neoselachii) beschrieben. Für die Charakterisierung derWurzelmorphologie synechodontiformer Zähne wird der Begriff „polyhemiaulacorhiz“ an Stelle des irreführenden älteren Terminus „pseudopolyaulacorhiz“ eingeführt. Die Zähne von Parascylloides turnerae gen. nov. sp. nov. wurden zuvor als Symphysenoder Parasymphysenzähne von Rhomphaiodon minor (Agassiz, 1837) angesprochen, werden hier jedoch aufgrund ihrer Häufigkeit und morphologischen Eigenart einer neuen Haiart zugeordnet. Der Zahnschmelz ist in beiden neuen Arten dreilagig aufgebaut und besteht aus einer äußeren Glanzschicht (SLE), einemmittleren parallelfaserigen Schmelz (PBE) und einem inneren wirrfaserigen Schmelz (TBE). Der parallelfaserige Schmelz zeigt in beiden Arten vertikale, oberflächenparallele Fasern aus Apatit-Kristalliten. Während im PBE von Synechodus seinstedtensis sp. nov. wahrscheinlich auch radiale Faserzüge vorhanden sind, fehlen diese im PBE von Parascylloides turnerae gen. nov. sp. nov. Die systematische Bedeutung des Vorhandenseins oder Fehlens von radialen Faserzügen im PBE, ein Phänomen, das auch bei anderen triassischen Neoselachiern beobachtet werden kann, bleibt unklar.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"01 1","pages":"137-167"},"PeriodicalIF":2.7,"publicationDate":"2014-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"86501041","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Evolutionary patterns of early and middle Aragonian (Miocene) of Megacricetodon (Rodentia, Mammmalia) from Spain","authors":"A. Pérez, P. Peláez-Campomanes","doi":"10.1127/PALA/303/2014/85","DOIUrl":"https://doi.org/10.1127/PALA/303/2014/85","url":null,"abstract":"This research was supported by the MICIIN, Project No. CGL2008-04200/BTE and CGL20 11-28877.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"19 1","pages":"85-135"},"PeriodicalIF":2.7,"publicationDate":"2014-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"85159901","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Systematic and palaeoecology of Psychodidae (Insecta: Diptera) from Miocene Mexican amber","authors":"Frauke Stebner, M. S. Kraemer","doi":"10.1127/PALA/303/2014/1","DOIUrl":"https://doi.org/10.1127/PALA/303/2014/1","url":null,"abstract":"","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"41 1","pages":"1-21"},"PeriodicalIF":2.7,"publicationDate":"2014-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"85752749","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2014-11-06DOI: 10.1127/PALA/303/2014/23
A. Athanassiou, S. Roussiakis, I. Giaourtsakis, G. Theodorou, G. Iliopoulos
The Late Miocene locality of Kerassia (North Euboea, Greece) has yielded a rich Turolian fauna, which forms part of the Eastern Mediterranean Pikermian biome. A prominent specimen of the Kerassia collection, a well-preserved rhinocerotid skull with associated mandible, is described herein. The specimen demonstrates the diagnostic cranial, mandibular, and dental characters of the genus Acerorhinus, but it is distinct enough in several anatomical aspects from the known samples of this genus to justify the establishment of a new species, A. neleus. It is characterised by the absence of horns, dolichocephaly, a moderately concave dorsal cranial profile, closely converging parietal crests, a relatively high-positioned orbit, a markedly robust zygomatic arch, a bell-shaped occipital outline, and a robust mandible. Its strong but relatively narrow mandibular symphysis has a short diastema, a concave ventral surface, and bears a pair of moderate-sized second lower incisors suggesting a female individual. The salient features of the upper dentition include a proportionally long premolar section and traces of a thin cement coating on the labial wall of the ectolophs. The upper premolars are characterised by the presence of a faint protocone constriction and a strong lingual cingulum, whereas the upper molars by the absence of lingual cinguli and the presence of a moderate protocone constriction. Clusters of numerous borings on the specimen’s surface were attributed to bioerosion induced by dermestid beetle activity. The Kerassia specimen is closely related to the few known aceratheriine specimens from Pikermi and Chomateri, which are described and referred to A. neleus n. sp. The taxonomic relationships among certain Eurasian aceratheriine samples are discussed and an updated systematic list of the Acerorhinus species is provided.
晚中新世的Kerassia地区(希腊Euboea北部)产生了丰富的图罗里亚动物群,构成了东地中海Pikermian生物群系的一部分。本文描述了Kerassia收藏的一个突出标本,一个保存完好的鼻颈颅骨和相关的下颌骨。该标本显示了针毛猴属的颅骨、下颌和牙齿的诊断特征,但它在几个解剖方面与该属的已知样本有足够的不同,足以证明建立一个新种a . neeleus。其特征是没有角,头多畸形,颅背轮廓中度凹,顶骨紧密汇聚,眼眶位置相对较高,颧弓明显强健,枕部轮廓呈钟形,下颌骨强健。它强壮但相对狭窄的下颌联合有一个短的间隙,一个凹的腹面,并有一对中等大小的第二下门牙,表明它是一个雌性个体。上牙列的显著特征包括成比例的长前磨牙部分和生态窝唇壁上薄水泥涂层的痕迹。上前磨牙的特征是存在微弱的原锥体收缩和强烈的舌带,而上磨牙的特征是没有舌带和存在适度的原锥体收缩。标本表面的大量钻孔归因于皮蝇甲虫活动引起的生物侵蚀。Kerassia标本与来自Pikermi和Chomateri的少数已知的针叶螨标本有密切的关系,它们被描述为A. neeleus n. sp.。讨论了欧亚大陆某些针叶螨标本之间的分类关系,并提供了一份更新的系统的针叶螨物种清单。
{"title":"A new hornless rhinoceros of the genus Acerorhinus (Perissodactyla: Rhinocerotidae) from the Upper Miocene of Kerassiá (Euboea, Greece), with a revision of related forms","authors":"A. Athanassiou, S. Roussiakis, I. Giaourtsakis, G. Theodorou, G. Iliopoulos","doi":"10.1127/PALA/303/2014/23","DOIUrl":"https://doi.org/10.1127/PALA/303/2014/23","url":null,"abstract":"The Late Miocene locality of Kerassia (North Euboea, Greece) has yielded a rich Turolian fauna, which forms part of the Eastern Mediterranean Pikermian biome. A prominent specimen of the Kerassia collection, a well-preserved rhinocerotid skull with associated mandible, is described herein. The specimen demonstrates the diagnostic cranial, mandibular, and dental characters of the genus Acerorhinus, but it is distinct enough in several anatomical aspects from the known samples of this genus to justify the establishment of a new species, A. neleus. It is characterised by the absence of horns, dolichocephaly, a moderately concave dorsal cranial profile, closely converging parietal crests, a relatively high-positioned orbit, a markedly robust zygomatic arch, a bell-shaped occipital outline, and a robust mandible. Its strong but relatively narrow mandibular symphysis has a short diastema, a concave ventral surface, and bears a pair of moderate-sized second lower incisors suggesting a female individual. The salient features of the upper dentition include a proportionally long premolar section and traces of a thin cement coating on the labial wall of the ectolophs. The upper premolars are characterised by the presence of a faint protocone constriction and a strong lingual cingulum, whereas the upper molars by the absence of lingual cinguli and the presence of a moderate protocone constriction. Clusters of numerous borings on the specimen’s surface were attributed to bioerosion induced by dermestid beetle activity. The Kerassia specimen is closely related to the few known aceratheriine specimens from Pikermi and Chomateri, which are described and referred to A. neleus n. sp. The taxonomic relationships among certain Eurasian aceratheriine samples are discussed and an updated systematic list of the Acerorhinus species is provided.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"213 1","pages":"23-59"},"PeriodicalIF":2.7,"publicationDate":"2014-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"74159156","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2014-11-06DOI: 10.1127/PALA/303/2014/61
K. Bastl, Doris Nagel, S. Peigné
Themilk dentition of the three known small-sized European species ofHyaenodon (Hyaenodon rossignoli – Eocene,Hyaenodon filholi and H. exiguus – both Oligocene) is described in detail, especially DP3, DP4 and the dp3 and dp4. Interspecific differences in the morphology of these teeth are noted.Themorphology ofHyaenodon filholi is similar to that of Asian andNorth American species and thus suggests this species is an Asian immigrant. According to this study, Hyaenodon exiguus is more distantly related to North American and Asian species than H. filholi. The presence and evolution of a European lineage in the Oligocene is evidenced for the first time.
{"title":"Milk tooth morphology of small-sized Hyaenodon (Hyaenodontidae, Mammalia) from the European Oligocene – evidence of a Hyaenodon lineage in Europe","authors":"K. Bastl, Doris Nagel, S. Peigné","doi":"10.1127/PALA/303/2014/61","DOIUrl":"https://doi.org/10.1127/PALA/303/2014/61","url":null,"abstract":"Themilk dentition of the three known small-sized European species ofHyaenodon (Hyaenodon rossignoli – Eocene,Hyaenodon filholi and H. exiguus – both Oligocene) is described in detail, especially DP3, DP4 and the dp3 and dp4. Interspecific differences in the morphology of these teeth are noted.Themorphology ofHyaenodon filholi is similar to that of Asian andNorth American species and thus suggests this species is an Asian immigrant. According to this study, Hyaenodon exiguus is more distantly related to North American and Asian species than H. filholi. The presence and evolution of a European lineage in the Oligocene is evidenced for the first time.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"133 1","pages":"61-84"},"PeriodicalIF":2.7,"publicationDate":"2014-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"75038465","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2014-02-21DOI: 10.1127/PALA/301/2014/63
Wagih S. Ayoub-Hannaa, F. Fürsich, G. M. Qot
68 bivalve species belonging to 13 orders, 29 families, and 51 genera, are systematically described from three Cenomanian-Turonian sections (Gebel Areif El-Naqa, East Themed, and Wadi Quseib) on the eastern side of the Sinai Peninsula. The stratigraphic range and palaeogeographic distribution is given for each species. Nine species are reported from Egypt for the first time. Due to their taxonomic relevance, the microstructure of the rudist taxa has been illustrated. The bivalve fauna strongly resembles that of other Tethyan regions in southern Europe, North Africa, Middle East, and eastern South America. Therefore, most of the identified taxa have a strong Tethyan affinity. The distribution patterns of bivalves have probably been influenced by east-west directed currents during the Cenomanian. However, due to the presence of geographic barriers, extensive shallow marine shelf areas, and narrowing of the Tethys during that time, the current split up, one branch extending in a clockwise direction to southeastern Europe. The opening of the Trans-Saharan Seaway of southern Tethyan bivalves immigrated to western Africa and eastern South America.
{"title":"Cenomanian-Turonian bivalves from eastern Sinai, Egypt","authors":"Wagih S. Ayoub-Hannaa, F. Fürsich, G. M. Qot","doi":"10.1127/PALA/301/2014/63","DOIUrl":"https://doi.org/10.1127/PALA/301/2014/63","url":null,"abstract":"68 bivalve species belonging to 13 orders, 29 families, and 51 genera, are systematically described from three Cenomanian-Turonian sections (Gebel Areif El-Naqa, East Themed, and Wadi Quseib) on the eastern side of the Sinai Peninsula. The stratigraphic range and palaeogeographic distribution is given for each species. Nine species are reported from Egypt for the first time. Due to their taxonomic relevance, the microstructure of the rudist taxa has been illustrated. The bivalve fauna strongly resembles that of other Tethyan regions in southern Europe, North Africa, Middle East, and eastern South America. Therefore, most of the identified taxa have a strong Tethyan affinity. The distribution patterns of bivalves have probably been influenced by east-west directed currents during the Cenomanian. However, due to the presence of geographic barriers, extensive shallow marine shelf areas, and narrowing of the Tethys during that time, the current split up, one branch extending in a clockwise direction to southeastern Europe. The opening of the Trans-Saharan Seaway of southern Tethyan bivalves immigrated to western Africa and eastern South America.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"65 1","pages":"63-168"},"PeriodicalIF":2.7,"publicationDate":"2014-02-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"74794311","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"A Systematic, Biostratigraphic, and Paleobiogeographic Reevaluation of the Siwalik Hipparionine Horse Assemblage from the Potwar Plateau, Northern Pakistan","authors":"D. Wolf, R. Bernor, T. Hussain","doi":"10.1127/PALA/300/2013/1","DOIUrl":"https://doi.org/10.1127/PALA/300/2013/1","url":null,"abstract":"","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"81 1","pages":"1-115"},"PeriodicalIF":2.7,"publicationDate":"2013-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77656991","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
M. Harzhauser, T. Neubauer, M. Gross, Herbert Binder
We present the first thorough revision of the continental mollusc fauna from the early Middle Miocene wetlands of the Rein Basin (Styria, Austria). Lake Rein was a shallow ephemeral lake with carbonate sedimentation. Its mollusc assemblage comprises 13 species and is dominated by planorbid gastropods in species and individual numbers, accompanied by lymnaeids and rare hydrobiids. The terrestrial assemblage consists of 35 species with Discidae, Elonidae and Helicidae as most abundant taxa along with carychiids. The terrestrial gastropods suggest moist woodland and only limited areas of open habitats; the freshwater species point to stagnant and shallow water bodies with dense vegetation and only very limited fluvial input. Many taxa are illustrated for the first time and historical mis-identifications are corrected. About one third of the species is known so far from the Rein Basin only, but the majority of the species is also known from other Middle Miocene lakes and wetlands of Central Europe. The strongest faunistic relations are indicated with the Badenian wetlands of the Paratethys Sea and the so-called Silvana-beds of Southern Germany. Hauffenia mandici Neubauer & Harzhauser n. sp., Radix enzenbachensis Neubauer & Harzhauser n. sp., Gyraulus krohi Neubauer & Harzhauser n. sp., Truncatellina pantherae Harzhauser & Neubauer n. sp., Euconulus styriacus Harzhauser, Neubauer & Binder n. sp., “Discus” schneideri Harzhauser & Neubauer n. sp. and Musculium miocaenicum Neubauer & Harzhauser n. sp. are introduced as new species. Cochlodina (Miophaedusa) reinensis Harzhauser & Neubauer n. nom. is introduced as replacement name for Clausilia gobanzi Penecke, 1891 non Pfeiffer, 1868.
本文首次对奥地利施蒂里亚Rein盆地中中新世早期湿地的陆生软体动物区系进行了全面的修正。雷小山湖为碳酸盐岩沉积的浅生湖。软体动物有13种,种类和个体数量以腹足类为主,伴以淋巴类和稀有的水螅类。陆生群落共有35种,以姬蝇科、姬蝇科和姬蝇科为最丰富的分类群。陆生腹足类表明潮湿的林地和有限的开放栖息地;淡水物种指向有茂密植被和只有非常有限的河流输入的停滞和浅水体。许多分类群是第一次插图,并纠正了历史上的错误识别。到目前为止,大约三分之一的物种只在雷小山盆地被发现,但大多数物种也在中欧的其他中新世中期湖泊和湿地被发现。在帕拉提提斯海的巴登尼亚湿地和德国南部所谓的西尔瓦纳河床中,显示出最强的动物群关系。作为新种引进的品种有:manffenia mandici Neubauer & Harzhauser n. sp、enzenbachensis Neubauer & Harzhauser n. sp、Gyraulus krohi Neubauer & Harzhauser n. sp、Truncatellina pantherae Harzhauser & Neubauer n. sp、Euconulus styriacus Harzhauser & Neubauer n. sp、“Discus”schneideri Harzhauser & Neubauer n. sp、muscuum miocaenicum Neubauer & Harzhauser n. sp。Cochlodina (Miophaedusa) reinensis Harzhauser & Neubauer n. nom.作为Clausilia gobanzi Penecke(1891)的替代名称引入,non Pfeiffer, 1868。
{"title":"The early Middle Miocene mollusc fauna of Lake Rein (Eastern Alps,Austria)","authors":"M. Harzhauser, T. Neubauer, M. Gross, Herbert Binder","doi":"10.1127/PALA/302/2013/1","DOIUrl":"https://doi.org/10.1127/PALA/302/2013/1","url":null,"abstract":"We present the first thorough revision of the continental mollusc fauna from the early Middle Miocene wetlands of the Rein Basin (Styria, Austria). Lake Rein was a shallow ephemeral lake with carbonate sedimentation. Its mollusc assemblage comprises 13 species and is dominated by planorbid gastropods in species and individual numbers, accompanied by lymnaeids and rare hydrobiids. The terrestrial assemblage consists of 35 species with Discidae, Elonidae and Helicidae as most abundant taxa along with carychiids. The terrestrial gastropods suggest moist woodland and only limited areas of open habitats; the freshwater species point to stagnant and shallow water bodies with dense vegetation and only very limited fluvial input. Many taxa are illustrated for the first time and historical mis-identifications are corrected. About one third of the species is known so far from the Rein Basin only, but the majority of the species is also known from other Middle Miocene lakes and wetlands of Central Europe. The strongest faunistic relations are indicated with the Badenian wetlands of the Paratethys Sea and the so-called Silvana-beds of Southern Germany. Hauffenia mandici Neubauer & Harzhauser n. sp., Radix enzenbachensis Neubauer & Harzhauser n. sp., Gyraulus krohi Neubauer & Harzhauser n. sp., Truncatellina pantherae Harzhauser & Neubauer n. sp., Euconulus styriacus Harzhauser, Neubauer & Binder n. sp., “Discus” schneideri Harzhauser & Neubauer n. sp. and Musculium miocaenicum Neubauer & Harzhauser n. sp. are introduced as new species. Cochlodina (Miophaedusa) reinensis Harzhauser & Neubauer n. nom. is introduced as replacement name for Clausilia gobanzi Penecke, 1891 non Pfeiffer, 1868.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"26 1","pages":"1-71"},"PeriodicalIF":2.7,"publicationDate":"2013-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90975812","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2013-10-14DOI: 10.1127/PALA/300/2013/117
M. Venczel, J. Hír
Seven localities from the Felsőtárkány Basin, N-Hungary, yielded at least 38 lissamphibian and squamate reptile taxa and represents to date one of the richest herpetofaunas from the middle/late Miocene of the Pannonian basin. The fossil assemblages with relatively high local diversity were deposited near the margins of the former Pannonian Sea in a wide variety of sedimentary environments. The composition of the fauna documents for a number of taxa (e.g., Albanerpetontidae indet., Salamandrina, Triturus cf. marmoratus, Lissotriton, Ophisaurus, Pseudopus, ‘Coluber’ pouchetii) a distinctly wider distribution during the Middle Miocene of continental Europe. On the other hand, several newcomers indicate (e.g., Parahynobius, Mertensiella cf. caucasica, Albaneryx cf. volynicus, Natrix cf. rudabanyaensis, Hierophis cf. hungaricus, Vipera berus complex), similarly to micromammals, an amplified faunal influence from the Asiatic continent. The fossil record of the land salamander genus Parahynobius (Hynobiidae) represents its first appearance date (FAD) in Europe, whereas those of Mertensiella, Salamandrina, Chalcides, Albaneryx and Vipera berus complex is the FAD in the Pannonian basin. Furthermore, the presence of the African-derived skink Chalcides indicates an earlier divergence history for this group of lizards. The estimated mean annual precipitation (MAP), based on the co-occurrences of certain lissamphibian and squamate taxa indicates a rising tendency across the Astaracian/Vallesian boundary and largely correlates with the estimations based on macrofloral associations.
{"title":"Amphibians and Squamates from the Miocene of Felsőtárkány Basin, N-Hungary","authors":"M. Venczel, J. Hír","doi":"10.1127/PALA/300/2013/117","DOIUrl":"https://doi.org/10.1127/PALA/300/2013/117","url":null,"abstract":"Seven localities from the Felsőtárkány Basin, N-Hungary, yielded at least 38 lissamphibian and squamate reptile taxa and represents to date one of the richest herpetofaunas from the middle/late Miocene of the Pannonian basin. The fossil assemblages with relatively high local diversity were deposited near the margins of the former Pannonian Sea in a wide variety of sedimentary environments. The composition of the fauna documents for a number of taxa (e.g., Albanerpetontidae indet., Salamandrina, Triturus cf. marmoratus, Lissotriton, Ophisaurus, Pseudopus, ‘Coluber’ pouchetii) a distinctly wider distribution during the Middle Miocene of continental Europe. On the other hand, several newcomers indicate (e.g., Parahynobius, Mertensiella cf. caucasica, Albaneryx cf. volynicus, Natrix cf. rudabanyaensis, Hierophis cf. hungaricus, Vipera berus complex), similarly to micromammals, an amplified faunal influence from the Asiatic continent. The fossil record of the land salamander genus Parahynobius (Hynobiidae) represents its first appearance date (FAD) in Europe, whereas those of Mertensiella, Salamandrina, Chalcides, Albaneryx and Vipera berus complex is the FAD in the Pannonian basin. Furthermore, the presence of the African-derived skink Chalcides indicates an earlier divergence history for this group of lizards. The estimated mean annual precipitation (MAP), based on the co-occurrences of certain lissamphibian and squamate taxa indicates a rising tendency across the Astaracian/Vallesian boundary and largely correlates with the estimations based on macrofloral associations.","PeriodicalId":56099,"journal":{"name":"Palaeontographica Abteilung A-Palaozoologie-Stratigraphie","volume":"24 1","pages":"117-158"},"PeriodicalIF":2.7,"publicationDate":"2013-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"84980365","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}